Kone (volcano)
| Kone | |
|---|---|
 Kone Volcano captured from Space. | |
| Highest point | |
| Elevation | 1,619 m (5,312 ft)[1] |
| Geography | |
  Kone | |
| Geology | |
| Mountain type | Calderas |
| Last eruption | 1820 ± 10 years[1] |
Kone is a volcano located in the Oromia region of Ethiopia. It is located on the Main Ethiopian Rift, which belongs to the most northern branch of the East African Rift Valley.[2] Borchotto the nearest town is 5 km away and the capital of Ethiopia, Addis Ababa is situated 160 km west of Kone. The nearest volcano is Fentale located 30 km to the North West, with the Boseti Gudo Volcano further away to the South East.[2] Kone takes up an area of 250 square miles and has an elevation of 1619m.[3]
History of eruptions
The complex tectonic history within Ethiopia has made the eruption history difficult to interpret from the Stratigraphic sequence. From the stratigraphy four volcanic sequences of eruption can be determined.[4] Three Silicic phases and then a basalt phase. The most recent basalt phase is dated around 1820. This date corresponds to local legends of the eruption and the lack of vegetation growth on the lava flows provides evidence of this eruption.
Geology
Kone, also called Gariboldi, is made up of seven nested calderas, lava flows and basaltic cinder cones. (Not to be confused with the Garibaldi Volcanic Belt in Northern America.) There are two fault lines that have caused the volcanic activity within Kone, normal faults, which are part of the Wonji fault belt and ring fractures. The normal faults cause magma to rise inducing the volcanic activity. The ring fractures have caused the calderas collapse. Both of these faults have caused activity within Kone’s recent history. The calderas widths can range from 1.5 to 5 km.
There are many rock types identified at Kone and they are divided into five main groups, trachytes, comenditic rhyolites, ignimbrites, pumices, syenite inclusions and basalts. Trachytes and comenditic rhyolites form the main volume of the rock in the Complex. The ignimbrites have formed massive green sheets ranging in thickness from 15 cm to 25 m. The pumice deposits over the ground are common within Kone’s Volcanic Complex and range in thickness from 50 cm to 20 m. Most of the pumice is found interlocked with the ignimbrites. There have been three basalt lava types identified at Kone,[5] aphyric basalt, olivine basalt and a third basalt which contains large phenocrysts of olivine, augite and plagioclase. These different rock types provide evidence for different eruptive phases. Kone is unusual due to the number of calderas in the Volcanic Complex, Fentale contains only one calderas in comparison.
Renaming
Kone’s name is a recent addition taken from a local tribal word. The historical name of Kone was Gariboldi. Named according to local legend after an engineer who was responsible for building a road through two of the collapsed calderas. Thereby connecting Addis Ababa to Djibouti during the Italian occupation of Ethiopia during the 1940s.[6]
References
- ^ a b c "Kone". Global Volcanism Program. Smithsonian Institution. Retrieved 2012-05-01.
- ^ a b Cole, J.W. (1969) Gariboldi Volcanic Complex, Ethiopia. Bulletin of Volcanology.33:566-578
- ^ "Kone Volcano, Ethiopia - John Seach". Volcanolive.com. Retrieved 2013-11-08.
- ^ Acocella. V, Korme. T, Salvini. Funciello. R (2002) Elliptic calderas in the Ethiopian Rift: control of pre-existing structures. Journal of Volcanology and Geothermal Research. 119:189-203
- ^ Cole, J.W. (1969) Gariboldi Volcanic Complex, Ethiopia. Bulletin of Volcanology. 33:566-578
- ^ "Kone | Volcano World". Volcano.oregonstate.edu. Retrieved 2013-11-08.